Submergent landforms Flashcards
what is a submerged landform?
= rapid increase in global temperature-> melting of ice, decreasing water stored in glaciers -> increase volume in sea as molecules expand. SL rise= FLANDRIAN TRANSGRESSION means landforms are found below the water surface
What is a fjord
= submerged glacial valley, up to 1km deep, 2-4km wide
-water sits in U-shaped valley formed by glaciation
-STEEP valley sides
-LONG with a ‘threshold’ at end (former terminal moraine)
Example of a fjord
Signed fjord in Norway- used by submarines!
How is a fjord formed?
- valley is formed by plucking and abrasion of glacier
- created by eustatic change after ice age where glacier melts and SL significantly rises
- this fills the glacial valley with meltwater
-coastal erosion at current SL widens fjords and forms notches (fairly insignificant as hard rock type slow to erode)
-rivers and waterfalls in hanging valleys slowly build up fjords by depositing sediment
-biological and freeze-thaw on sides create scree
what is a ria?
= through lowland coastal areas rivers form floodplains and deltas made of alluvial deposits (silts and clay) due to flocculation
example of a ria/ key features
South coast of Devon, Saltcombe and dartmouth
-flooded tributaries/exposed smooth valley sides
-sheltered coastal location used for shipping and settlements=> people develop defences to protect => alter coastal processes
How is a ria formed?
- SL rise floods floodplains -> shallow and wide bodies of water with one narrow old river section
- due to large tidal range-> inlets and mudflats created for wildlife
what is a shingle beach
=long beaches with large quantities of glacial sediment (greater than what’s provided by cliff erosion)
example of a shingle beach/ dominant processes
Chesil peach/porlock bay
-LSD alters beach profile massively
-eustatic rise can flood beach in LY
-human interventions slow LSD
how are shingles beaches formed?
- sediment ‘rolled up’ from offshore as SL rise during Flandrian Transgression 10-6000 years ago=> causes wave action to push sediment onshore
- SL increase further erodes cliffs-> pushing newley-created sediment along the glacially deposited sediment further inland